Central cantabrian valleys. Patterns of evolution according to different time-scales

被引：0
作者：
Frochoso Sanchez, Manuel [1 ]
机构：
[1] Univ Cantabria, Urbanismo Ordenac Territorio, Dept Geografia, Santander, Spain
来源：
ERIA-REVISTA CUATRIMESTRAL DE GEOGRAFIA | 2016年 / 99-100期
关键词：
Mountain; erosional processes; morphogenesis of the valleys; Central Cantabrian Mountains; northern Spain;
D O I：
暂无
中图分类号：
P9 [自然地理学]; K9 [地理];
学科分类号：
0705 ; 070501 ;
摘要：
The valley is the basic landform unit in the cantabrian landscape and we use different time-scales in their explanation. First, the time of the origin of valleys, with the tectonic/erosion interaction (millions of years). Second, the time of the shape of the valleys due to the climatic crisis (hundreds of thousands of years). By last, the time of the reshape of the slopes and thalwegs (thousands of years and centuries).
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页码：71 / 91
页数：21
相关论文
共 80 条
  • [1] Glaciers and rivers: Pleistocene uncoupling in a Mediterranean mountain karst
    Adamson, K. R.
    Woodward, J. C.
    Hughes, P. D.
    [J]. QUATERNARY SCIENCE REVIEWS, 2014, 94 : 28 - 43
  • [2] Alfonso Gomez A., 1973, CUADERNOS ESPELEOLOG, P119
  • [3] Alonso-Zarza A. M., 2002, GEOLOGY SPAIN, P293
  • [4] Ballantyne C., 2002, QUATERNARY SCI REV
  • [5] BARRIENDOS Mariano, 2009, DESASTRE NATURAL VID, P253
  • [6] Bertrand C., 1984, TRAVAUX RGPSO, P247
  • [7] Bertrand G., 1971, REV GEOGRAPHIQUE PYR, V42, P49, DOI [10.3406/rgpso.1971.4872, DOI 10.3406/RGPSO.1971.4872]
  • [8] Boillot G., 1980, B BRGM, P93
  • [9] Castanon J. C., 1998, PROCESOS BIOFISICOS, P113
  • [10] Castanon J. C., 1989, THESIS
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